高壓熱水供暖 的英文怎麼說
中文拼音 [gāoyārèshuǐgōngnuǎn]
高壓熱水供暖
英文
high-pressure hot water heating- 高 : Ⅰ形容詞1 (從下向上距離大; 離地面遠) tall; high 2 (在一般標準或平均程度之上; 等級在上的) above...
- 壓 : 壓構詞成分。
- 水 : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
- 供 : 供Ⅰ名詞1 (供品) offerings 2 (口供; 供詞) confession; deposition Ⅱ動詞1 (供奉) lay (offerin...
- 暖 : Ⅰ形容詞(暖和) warm; genial Ⅱ動詞(使東西變熱或使身體變溫暖) warm up
- 高壓 : 1 (殘酷迫害; 極度壓制) high handed 2 [氣象學] (高氣壓) high pressure3 (高電壓) high tension...
- 熱水 : hot water熱水袋 hot water bog; hot water bottle; 熱水供[采]暖 [機械工程] hot water heating; hydra...
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We can use the mm5 model in definite time, definite area weather forecasting. we conclude that : : the moving route of this necw in its developing progress was direct - south along latitude, the cold air is rough, and just this made the rough vertical velocity ; the necw southern moving and conflicting with the west pacification sub - tropical high makes rough jet steam. the plenty south - west warm and wet air made by the jet stream gave the rainstorm demanded vapor ;. the rough vertical velocity by jet stream is a main reason in this rainstorm ; the mm5 model uses four - direction analysis data as its input, this avoids some errors occurred in observe and transfer, thus made the result more useful
綜合分析認為: ( 1 ) 、這次冷渦在其發生發展過程中,其移動路徑是沿經圈直線南壓,攜帶的冷空氣勢力較強,形成槽后較強的垂直運動; ( 2 ) 、西太平洋副熱帶高壓偏北位置與東北冷渦南壓形成的急流軸,把源源不斷的西南暖濕氣流輸送到遼西地區,也就是急流軸的左前方位置,為這次暴雨的產生提供了充足的水汽來源; ( 3 ) 、低空急流不但為暴雨輸送水汽,其造成的較強的垂直環流也是產生強降水的一個主要原因; ( 4 ) 、 mm5模式以四維同化資料作為初始場,最大限度地避免了觀測誤差可能造成的積分不穩定,提高了模擬結果的參考價值。Environment protection becoming a focus in big cities, to meet the energy needs mainly by clean energy products is a prevailing trend. to promote energy conservation, heating system and charge policy is facing great reform. air - conditioner becoming necessity, the city electricity supply systems are confronted by peak load
當前我國大城市關注環保問題,城市能源結構調整勢在必行;民用供暖「分戶計量按熱取費」制度的建立與實現,是調動用戶節能積極性實現供暖節能目標的關鍵之所在;伴隨居民生活水平的提高,空調迅速普及給城市電網帶來巨大壓力。The article point out that the downward transport of the high moist potential vorticity from high level causes the development of low level cyclone. the rainfall may occur near the south area of positive center of mpv1 and negative region of mpv2 at 500hpa
在整個降水過程中,副熱帶高壓穩定少動,其西北側的暖濕氣流為強降水提供了充沛的水汽條件,地面冷鋒和高原低渦是其抬升機制。
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